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6 - Fault Identification from Seismology
from Part II - Methods and Techniques for Fault Identification and Dating
- By Nicolai Gestermann, Thomas Plenefisch
Edited by Holger Steffen, Odleiv Olesen, Raimo Sutinen
Book:

Glacially-Triggered Faulting

Published online:

02 December 2021

Print publication:

16 December 2021, pp 100-117
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Summary

Regions affected by glacial isostatic adjustment experience stress changes. The stress will be released either by slow aseismic movements along faults or by sudden stress release in form of earthquakes. Location and source mechanism of those earthquakes can play a major role in understanding past and ongoing geodynamic processes in a glacial isostatic adjustment-affected region. On the one hand, alignments of earthquake hypocentres may act as an indicator for active faults that might not be known from geology before. On the other hand, calculation and interpretation of earthquake focal mechanisms, represent a key to stress and stress changes. We present an overview of seismological methods and tools to retrieve fault geometry and motion.